Soil and Unsaturated Flow
External reference: https://openalex.org/T10716
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Water Adsorption of Non-Saline and Salt-Affected Clay
Water vapor adsorption in salt-affected clays varies with humidity, with salinity enhancing uptake at high relative humidity through capillary condensation.
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Temporal linearization can bias root water uptake estimates
Temporal linearization approximations for estimating root water uptake from soil-water flux gradients fail under dynamic field conditions, introducing substantial systematic errors in hydraulic.
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Freeze–thaw reshapes water, salt, and heat in saline farmland soil
Freeze-thaw driven water-salt redistribution in saline farmland soils: quantified hydrothermal parameters and coupled migration mechanisms from field-laboratory verification.

